Two solutional caves are also reported to exist in this area.

There are a large number of solutional caves and rock shelters inside the cliff, but access is very difficult.

The largest and most abundant solutional caves are located in limestone.

They are typically formed in limestone or dolostone solutional caves.

The portions of a solutional cave that are below the water table or the local level of the groundwater will be flooded.

A solutional cave is a cave usually formed in soluble rock such as limestone.

As in solutional caves, small speleothems may develop in sea caves.

The limestone solutional cave is a National Natural Landmark.

Lechuguilla and nearby Carlsbad Cavern are now believed to be examples of another type of solutional cave.

Palaemonetes cummingi is endemic to a single flooded solutional cave in Alachua County, Florida.

Park caves, like most caves in the Sierra Nevada of California, are mostly solutional caves dissolved from marble.

Moaning Cavern is a solutional cave located near Vallecito, California in the heart of the state's Gold Country.

Elsewhere, in places such as Thailand's Phang Nga Bay, solutional caves have been flooded by the sea and are now subject to littoral erosion.

A small gypsum solutional cave, known as the Pellerito Cave (named after its founder, Russell Pellerito) was discovered during the mining operations.

This species has been reported from eight solutional caves in southern Leon County as well as six caves in Wakulla County, Florida.

Discovered by accident in 1881 by William Vanasse, Crystal Cave is a multi-level solutional cave formed in dolomite bedrock located in the Prairie du Chien grouping.

Solutional caves are the most frequently occurring caves and such caves form in rock that is soluble, such as limestone, but can also form in other rocks, including chalk, dolomite, marble, salt, and gypsum.

Cascade Caverns is a historically, geologically and biologically important limestone solutional cave located three miles south of Boerne, Texas, United States, on 226 Cascade Caverns Road, in Kendall County.

The Lena Hara cave is the main cave of a system of solutional caves in the Lautém District at the eastern tip of East Timor (Timor-Leste), close to the village of Tutuala.

While Maryland may be smaller than many of its neighboring states containing larger numbers of caves, its geology likewise allows for the formation of underground cavities, most of which are hollowed out by chemical processes-these caves are known as solutional caves.

Coastal Plain - this is the area of Maryland extending from just west of the Chesapeake Bay to the Atlantic Ocean: Precambrian rocks are mostly overlain by gravel, silts, marls, and sands, and consequently no solutional caves are known to exist in this region of Maryland.

The community is situated at the eastern base of South Mountain at elevations between 500-700'; the landscape here is principally underlain by the Tomstown Dolomite, and the neighboring area is home to at least four known solutional caves, one of which-Mount Aetna Cave-was open briefly for commercial tours in the 1930s.